WANG XingZhi, ZHANG Fan, MA Qing, YANG ManPing, WANG YiGang, WEN YingChu, YANG Yu, ZHANG Jing. The Characteristics of Reef and Bank and the Fluctuation of Sea-level in Feixianguan Period of Late Permian-Early Triassic,East Sichuan Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 249-254.
Citation:
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WANG XingZhi, ZHANG Fan, MA Qing, YANG ManPing, WANG YiGang, WEN YingChu, YANG Yu, ZHANG Jing. The Characteristics of Reef and Bank and the Fluctuation of Sea-level in Feixianguan Period of Late Permian-Early Triassic,East Sichuan Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 249-254.
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The Characteristics of Reef and Bank and the Fluctuation of Sea-level in Feixianguan Period of Late Permian-Early Triassic,East Sichuan Basin
- 1.
Sout hwest petroleuminstit ute, Nanchong,Sichuan 63700l;
- 2.
exploration and exploitation research instit ute of Sout hwest petroleum branch Campany, Chengdu 6l0050
- Received Date: 2000-11-23
- Rev Recd Date:
2001-05-03
- Publish Date:
2002-04-10
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Abstract
On the basis of the sedimentary characteristics and reservoir distribution law in Feixianguan Formation of Upper Permian-Lower Triassic,East Sichuan Basin, it can be determined that the characteristics and distribution of Changxin reefs and Feixiangguan oolitic banks are tighly relevent to the fluctuation of sea-level.The Changxin reefs developed during the rapid rising of sea-level on the ramp and inner ramp. When the growing speed of the reefs was lower than the rising one of sea-level,catch-up transgression reefs were formed,and when growing speed of the reefs was quicker than the rising one of sea-level,keep-up transgression reefs were formed.The Feixianguan oolitic banks were formed on the inner platform rim and some inner platform areas during the regression of sea-level, single platform rim banks were distributed widely and thickly,although the inner platform banks were of large number,they were thin and narrow in range.So,development formations of Changxin reefs rose towards transgression direction,and the Feixianguan oolitic banks migrated towards platform expandtion with regression. The Formation was deposited in a large scale of fluctuation of sea-level,the transgression begun in the early Wujiapin period, sea-level rose rapidly in the Changxin period ,and it reached summit in the early Feixianguan period,then lowered down in the following Feixianguan period until to the end of the time.
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Proportional views
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